Mössbauer Spectroscopy: Principles and Applications

 
 
James M. Byrne
University of Tuebingen
 
Discovered by Rudolf Mössbauer – 1958
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Used to:
Identify minerals
Determine redox state
Quantify relative abundancies of
different minerals in a sample
Determine crystallinity
 
Mössbauer Spectroscopy - Basics
 
Typically the data is described as:
Singlet
Doublet
Sextet
 
Technically speaking, the singlet, doublet and sextet
use the same equation, but people often find it
easier to describe them as being three distinct
types of spectra
 
Typical spectra
 
Typical spectra
 
https://serc.carleton.edu/research_education/geochemsheets/
techniques/mossbauer.html
 
Parameters
 
Coey J M D., 1974, Iron compounds in lake sediments
 
Fit the data using a Lorentzian function (Right figure).
The red line in the fitted figure simply corresponds to this lorentzian line.
 
Raw data
 
Raw data with a fitted line (Red)
 
Singlet
 
L(x)
=Transmission
x
 = velocity
Γ
 
= Linewidth (usually 0.097)
x0 
= distance from center
 
The Lorentzian lineshape equation is described by:
 
Transmission
 
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Singlet
 
Sometimes the data consists of two lines which are
joined together
 
Raw data
 
Raw data with a fitted line (Red)
 
Doublet
 
L(x)
=Transmission
x
 = velocity
Γ
 
= Linewidth (usually 0.097)
x01 
= distance from centre for the left curve
X02 = distance from centre for the right curve
 
For a doublet, the Lorentzian equation is just slightly modified:
 
Transmission
 
Here X01 and X02 contain the two most
important parameters called „center shift“ and
„quadrupole splitting“
 
Center shift = (x01 + x02)/2
Quadrupole splitting = x01+x02
 
Doublet
 
Develop an 
online data fitting tool 
where people
can load Mössbauer data, fit the data and obtain
the important information to interpret the data
 
To make it easier for people to learn Mössbauer
So we can increase the >100 groups using it to >1000
 
Short Term Goals
 
www.mosstool.com
 
Go to the website now
 
What happens in the background?
 
www.mosstool.com
 
1.
Develop a 
general data analysis website 
where people
using many different types of technique (not just
Mössbauer) can upload their data and easily fit it.
 
2.
Have 
a support system 
where researchers can get advice
from community experts (like a webchat or forum)
 
3.
Be able to easily 
identify a scientist who has expertise 
a
certain technique and can do measurements for other
external groups.
 
Long Term Goals
 
www.mosstool.com
 
Maybe we could have a front end where people can work with and teach all sorts of different
type of online data fitting tools?
 
Future?
 
www.mosstool.com
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Mössbauer Spectroscopy is a technique discovered by Rudolf Mössbauer in 1958, based on the recoilless emission and absorption of gamma radiation. It is used to identify minerals, determine redox states, quantify mineral abundancies, and assess crystallinity. The method involves analyzing typical spectra, fitting data using Lorentzian functions, and deriving parameters like center shifts. This analytical tool has been utilized in various fields, including studying iron compounds in lake sediments. The technique is powerful in providing detailed information through singlets, doublets, and sextets in the spectra, offering valuable insights into material properties.

  • Mössbauer Spectroscopy
  • Rudolf Mössbauer
  • Mineral Analysis
  • Gamma Radiation
  • Lorentzian Function

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  1. James M. Byrne University of Tuebingen

  2. Mssbauer Spectroscopy - Basics Discovered by Rudolf M ssbauer 1958 Dependent upon recoil recoil- -less emission less emission and absorption of gamma radiation absorption of gamma radiation. Used to: Identify minerals Determine redox state Quantify relative abundancies of different minerals in a sample Determine crystallinity

  3. Typical spectra Typically the data is described as: Singlet Doublet Sextet Technically speaking, the singlet, doublet and sextet use the same equation, but people often find it easier to describe them as being three distinct types of spectra

  4. Typical spectra https://serc.carleton.edu/research_education/geochemsheets/ techniques/mossbauer.html

  5. Parameters Coey J M D., 1974, Iron compounds in lake sediments

  6. Singlet Velocity (mm/s) Velocity (mm/s) -4 -2 0 2 4 -4 -2 0 2 4 Raw data Raw data with a fitted line (Red) Fit the data using a Lorentzian function (Right figure). The red line in the fitted figure simply corresponds to this lorentzian line.

  7. Singlet The Lorentzian lineshape equation is described by: 1 2 ? ? =1 (? ?0)2+(1 ? 2 )2 Velocity (mm/s) -4 -2 0 2 4 L(x)=Transmission x = velocity = Linewidth (usually 0.097) x0 = distance from center Transmission x0 x0 provides the most information and referred to as a Parameter which in this case would be referred to as center shift .

  8. Doublet Velocity (mm/s) Velocity (mm/s) -12 -10 -8 -6 -4 -2 0 2 4 6 8 10 12 -12 -10 -8 -6 -4 -2 0 2 4 6 8 10 12 Raw data Raw data with a fitted line (Red) Sometimes the data consists of two lines which are joined together

  9. Doublet For a doublet, the Lorentzian equation is just slightly modified: 1 2 1 2 1 ? 2 )2+1 ? ? = ? ?????+ ? ???? ?= (? ?01)2+(1 (? ?02)2+(1 2 )2 ? Velocity (mm/s) L(x)=Transmission x = velocity = Linewidth (usually 0.097) x01 = distance from centre for the left curve X02 = distance from centre for the right curve -12 -10 -8 -6 -4 -2 0 2 4 6 8 10 12 Transmission Here X01 and X02 contain the two most important parameters called center shift and quadrupole splitting Center shift = (x01 + x02)/2 Quadrupole splitting = x01+x02

  10. Short Term Goals Develop an online data fitting tool where people can load M ssbauer data, fit the data and obtain the important information to interpret the data To make it easier for people to learn M ssbauer So we can increase the >100 groups using it to >1000

  11. www.mosstool.com Go to the website now

  12. What happens in the background? www.mosstool.com

  13. Long Term Goals 1. Develop a general data analysis website where people using many different types of technique (not just M ssbauer) can upload their data and easily fit it. 2. Have a support system where researchers can get advice from community experts (like a webchat or forum) 3. Be able to easily identify a scientist who has expertise a certain technique and can do measurements for other external groups. www.mosstool.com

  14. Future? Maybe we could have a front end where people can work with and teach all sorts of different type of online data fitting tools? www.mosstool.com

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